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Related Articles That May Interest You A reassessment of Iteravis huchzermeyeri and Gansus zheni from the Jehol Biota in western Liaoning, China Shu-bin Ju, Xu-ri Wang, Yi-chuan Liu, Yang Wang Citation: Shu-bin Ju, Xu-ri Wang, Yi-chuan Liu, Yang Wang, 2021. A reassessment ofIteravis huchzermeyeri and Gansus zheni from the Jehol Biota in western Liaoning, China, China Geology, 4, 197-204. doi: 10.31035/cg2020066. 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The detailed comparisons of the holotype and referred specimens of both Available online 24 November 2020 species, reveal no anatomical features that distinguish these taxa as separate species. Some minor differences are considered to relate to ontogenetic or interspecific differences. The stratigraphic occurrence Keywords: for both specimens is the Lower Cretaceous Jiufotang Formation. Accordingly, the authors conclude that Jehol Biota Iteravis huchzermeyeri has priority, by 15 days, for this taxon and that Gansus zheni is a junior synonym. Lower Cretaceous Ornithuromorpha The diagnosis of Iteravis huchzermeyeri is revised based on further study on all specimens referred to this Synonym species. Its generic distinction from Gansus is maintained thereby removing a potential genus-level Geological survey engineering correlation linking Xiagou Formation in Gansu Province with the Jiufotang Formation in Liaoning Western Liaoning Province. China ©2021 China Geology Editorial Office. 1. Introduction between the ilium and ischium. A large number of fossils of ornithuromorphs have been found in China preserved with not Ornithuromorpha is the most inclusive clade that includes only clear skeletal anatomical features, but also feathers, extant birds but not Mesozoic Enantiornithes (Chiappe LM, gastroliths and even skin impressions, which are significant 2002). As of July 2020, more than 20 species of for studying the origin, radiation and life habits of species in Ornithuromorpha have been reported from the Lower this clade (Zhou ZH and Zhang FC, 2001; You HL et al., Cretaceous in China, which are mostly distributed in the Jehol 2006; Chiappe LM et al., 2014; Zhou S et al., 2014; Wang M Biota in northern Hebei, western Liaoning and the et al., 2016; Zheng XT et al., 2018). neighboring areas of Inner Mongolia (Zhou ZH and Zhang Over the last 20 years, lots of new species of FC, 2001, 2005; Chiappe LM et al., 2014; Wang M et al., Ornithuromorpha have been coined based on specimens 2015). The characteristics that distinguish Ornithuromorpha uncovered from the Jehol Biota in China (e.g., Chaoyangia from other Mesozoic birds include the U-shaped furcula beishanensis, Yixianornis grabaui, Yanornis martini, Hongshanornis longicresta, Archaeorhynchus spathula, without hypocleideum, rectangular sternum with a keel, as Jianchangornis microdonta, Longicrusavis houi, Schizooura well as completely fused metatarsals. According to the lii, Piscivoravis lii, Iteravis huchzermeyeri, Gansus zheni, morphological characteristics, most species of this group have Tianyuornis cheni, Archaeornithura meemannae, strong flight abilities. Some species still retain primitive Changzuiornis ahgmi, Bellulia rectusunguis, Eogranivora features, such as the teeth, the pubic symphysis developed at edentulata, Khinganornis hulunbuirensis) (Hou LH and the distal end of the pubic bone, and no ilium ischial foramen Zhang J, 1993; Zhou ZH and Zhang FC, 2001, 2005, 2006; Zhou FC et al., 2009; O’Connor JK et al., 2010; Zhou S et al., First author: E-mail address: [email protected] (Shu-bin Ju). 2014; Liu D et al., 2014; 2018; Wang M et al., 2015, 2016; * Corresponding author: E-mail address: [email protected] (Xu-ri Wang). Huang JD et al., 2016; Wang XR et al., 2020). Because doi:10.31035/cg2020066 different researchers may study different specimens of the 2096-5192/© 2021 China Geology Editorial Office. same species more or less simultaneously, it is likely that 198 Ju et al. / China Geology 2 (2021) 197−204 synonyms of a single species could be published. Iteravis stratigraphic occurrence for I. huchzermeyeri should be the huchzermeyeri (Zhou S et al. 2014) and Gansus zheni (Liu D Lower Cretaceous Jiufotang Formation. et al. 2014) were both uncovered at Sihedang town, Lingyuan City, Liaoning Province. The former was reported from the 3. Description and comparison Yixian Formation and the latter was from the Jiufotang Formation. I. huchzermeyeri was published 15 days earlier The central axial lengths from head to tail for the holotype than G. zheni. Most importantly, they have very similar specimens of I. huchzermeyeri (IVPP V18958) and G. zheni characteristics and very close phylogenetic relationship (Zhou (BMNHC-Ph1342), and the referred specimens of G. zheni S et al., 2014; Liu D et al., 2014). Wang X et al. (2018) (BMNHC-Ph1318) are about 204.3 mm, 195.7 mm and 217 mm, proposed that G. zheni was a synonym of I. huchzermeyeri, respectively, showing a variation in body length of less than but they did not conduct detailed comparisons and discussion. 10%. Although no osteohistological analyses have been taken G. zheni provided the best-known example of genus-level for the studied materials, the well ossified periosteal surfaces avian clade correlation between two broadly separated basins of the preserved elements and the complete fusion of the (being closely related to Gansus yumenensis found about tibiotarsus and tarsometatarsus indicated that they all were 2000 km distant in the Xiagou Formation, Gansu Province) adults or near-adults that had ceased to grow (Zhou S et al., and represented the most advanced bird for the Jehol Biota 2014; Liu D et al., 2014). (Liu D et al., 2014). It is worthy to clarify its validity, horizon Skulls of IVPP V18958, BMNHC-Ph1342 and BMNHC- Ph1318 are sub-triangular in shape, with a long rostrum and relationship with I. huchzermeyeri and G. yumenensis. nearly half of the skull length. The distinct pores are present 2. Systematic Paleontology on the lateral surface of premaxilla of IVPP V18958, which might represent vascularization of the horny beak. Similar Aves Linnaeus C, 1758 pores are also present on the lateral surface of the premaxilla Ornithothoraces Chiappe LM, 1995 and maxilla of BMNHC-Ph1342. The dentaries of IVPP Ornithuromorpha Chiappe LM, 2002 V18958, BMNHC-Ph1342 and BMNHC-Ph1318 are Iteravis huchzermeyeri Zhou S et al., 2014 relatively straight, and their posterior ends are slightly curved Revised diagnosis: Premaxillary corpus elongate and towards the ventral sides. The distal end of the surangular is toothless; maxilla and dentary with numerous small teeth; deeply concave in IVPP V18958, while this part is not visible rostrum 50% of skull length; ethmoid bone lining rostral half in BMNHC-Ph1318 (Fig. 1). The frontal is overlapped by the of the orbit; sternal margin of the coracoid extended nearly radius of IVPP V18958. There is a narrow salt gland fossa on equally medially and laterally; rostral margin of the sternum the frontal of BMNHC-Ph1342, which is smaller and strongly arched, defining an acute angle slightly less than 90°; narrower than that of Ichthyornis and Hesperornis (Wang X et alular metacarpal short and narrow, slightly more than half the al., 2018). The teeth are present on both dentary and maxilla width of the major metacarpal; pubic strongly curved dorsally of IVPP V18958, with several teeth mutually intercalating. from the distal 1/3 and with dorsally expanded distal boot; However, very small teeth are only visible on the dentary of ischium with concave
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